{"pageNumber":"613","pageRowStart":"15300","pageSize":"25","recordCount":16497,"records":[{"id":68319,"text":"ha333 - 1970 - Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula","interactions":[],"lastModifiedDate":"2021-10-21T15:12:36.579623","indexId":"ha333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"333","title":"Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula","docAbstract":"<p>The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, and trout fishing), but the expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, for irrigation, and for the dilution of sewage and other wastes. In order to make intelligent decisions regarding use and management of the water resource for recreation and other demands, an analysis of the hydrologic factors related to recreational values is essential.</p><p>The Pigeon River is one of Michigan's outstanding trout streams and is the favorite of a large number of anglers who return year after year. Camping is also popular and is usually, but not always, associated with fishing. Boating is very rare on the Pigeon because of numerous portages around log jams. Cabin-living and resorting are relatively minor on this river as yet, but much of the private river front may be developed in future years.</p><p>The Pigeon is located in the north-central part of the southern peninsula of Michigan (see index map). Headwaters are a few miles northeast of Gaylord, and the mouth is at Mullet Lake, a few miles northeast of Indian River. Interstate Highway 75 roughly parallels the river about 5 to 10 miles to the west. Exits from this highway at Gaylord, Vanderbilt, Wolverine, and Indian River, provide easy access to the Pigeon.</p><p>The recreational value of the river depends on the streamflow characteristics, quality of water, and character of stream channel, and bed and banks. The purpose of this atlas is to describe these characteristics, and to show how they relate to recreational uses.</p><p>Most of the information presented here was obtained from a field reconnaissance in June, 1966, and from basic records of the U.S. Geological Survey's Water Resources Division. The area of field study is limited to the channel, bed, and banks of the main stem of the Pigeon from source to mouth. The study was made in cooperation with the Michigan Geological Survey, Gerald E. Eddy, Chief. Advice and assistance were also obtained from other sections of the Michigan Conservation Department.</p><p>Sheet 1 of this atlas presents information on streamflow characteristics and water quality. Sheet 2 describes the physical characteristics of the stream channel, and bed and banks, and shows how these physical characteristics relate to streamflow, water quality, and recreational use.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha333","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1970, Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula: U.S. Geological Survey Hydrologic Atlas 333, 5 Plates: 30.5 x 40.0 inches or smaller, https://doi.org/10.3133/ha333.","productDescription":"5 Plates: 30.5 x 40.0 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":185889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha333.JPG"},{"id":89776,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390726,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15708.htm"},{"id":89775,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89774,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89773,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89772,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Michigan","otherGeospatial":"Pigeon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.61666666666666,45.03333333333333 ], [ -84.61666666666666,45.43333333333333 ], [ -84.41666666666667,45.43333333333333 ], [ -84.41666666666667,45.03333333333333 ], [ -84.61666666666666,45.03333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63afc9","contributors":{"authors":[{"text":"Hendrickson, G. 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,{"id":67993,"text":"ha352 - 1970 - Flood of June 1967 at Grand Island, Nebraska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha352","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"352","title":"Flood of June 1967 at Grand Island, Nebraska","language":"ENGLISH","doi":"10.3133/ha352","usgsCitation":"Shaffer, F.B., and Braun, K.J., 1970, Flood of June 1967 at Grand Island, Nebraska: U.S. Geological Survey Hydrologic Atlas 352, 1 map., https://doi.org/10.3133/ha352.","productDescription":"1 map.","costCenters":[],"links":[{"id":186364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89236,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/352/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5,40.8675 ], [ -98.5,41 ], [ -98.25,41 ], [ -98.25,40.8675 ], [ -98.5,40.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eed61","contributors":{"authors":[{"text":"Shaffer, F. Butler","contributorId":8856,"corporation":false,"usgs":true,"family":"Shaffer","given":"F.","email":"","middleInitial":"Butler","affiliations":[],"preferred":false,"id":277467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braun, Kenneth J.","contributorId":21225,"corporation":false,"usgs":true,"family":"Braun","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277468,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68260,"text":"ha356 - 1970 - Water resources of the River Rouge basin, southeastern Michigan","interactions":[],"lastModifiedDate":"2022-02-09T22:40:00.911686","indexId":"ha356","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"356","title":"Water resources of the River Rouge basin, southeastern Michigan","docAbstract":"<p>The River Rouge basin is characterized by moderately hilly topography to the northwest graduating to a relatively level land surface to the south east.</p><p>Stream gradients near the northwestern basin divide are relatively steep; but many become more steep in reaches where they cross beach lines of former glacial lakes. In the lower reaches of the River Rouge gradients lessen.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha356","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Knutilla, R., 1970, Water resources of the River Rouge basin, southeastern Michigan: U.S. Geological Survey Hydrologic Atlas 356, Document: 12 p.; 2 Plates: 40.5 x 30.5 inches and 36.26 x 35.76 inches, https://doi.org/10.3133/ha356.","productDescription":"Document: 12 p.; 2 Plates: 40.5 x 30.5 inches and 36.26 x 35.76 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":395741,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15733.htm"},{"id":89657,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/356/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89656,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/356/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/356/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/356/report-thumb.jpg"}],"scale":"125000","country":"United States","state":"Michigan","otherGeospatial":"River Rouge basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.636,\n              42.224\n            ],\n            [\n              -83.636,\n              42.604\n            ],\n            [\n              -83.068,\n              42.604\n            ],\n            [\n              -83.068,\n              42.224\n            ],\n            [\n              -83.636,\n              42.224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602545","contributors":{"authors":[{"text":"Knutilla, R. L.","contributorId":65451,"corporation":false,"usgs":true,"family":"Knutilla","given":"R. L.","affiliations":[],"preferred":false,"id":277925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24491,"text":"ofr70294 - 1970 - Flood profile study, Hoosier Creek, Linn County, Iowa","interactions":[],"lastModifiedDate":"2016-02-22T11:32:13","indexId":"ofr70294","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-294","title":"Flood profile study, Hoosier Creek, Linn County, Iowa","docAbstract":"<p>The purpose of this report is to present the results of a flood-profile study made for Hoosier Creek and its tributary, South Hoosier Creek. The reaches studied extend from near the south Linn County line upstream to U.S. Highway 218 on Hoosier Creek, and from the mouth to U.S. Highway 218 on South Hoosier Creek. A total of about 11 miles of stream is included in the two reaches. The profiles shown in the report are computed for a very large flood under existing valley conditions and for a smaller flood under two assumed conditions of encroachment. This information can be used to supplement the existing county zoning ordinances for flood plains and to aid in future flood-plain management when part or all of the area is urbanized. This report is the result of a cooperative agreement between Linn County, Iowa, and the U.S. Geological Survey that provides for the collection and analysis of hydrologic data in Linn County.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/ofr70294","issn":"0094-9140","collaboration":"Prepared in cooperation with Linn County, Iowa","usgsCitation":"Schwob, H.H., 1970, Flood profile study, Hoosier Creek, Linn County, Iowa: U.S. Geological Survey Open-File Report 70-294, 80 p., https://doi.org/10.3133/ofr70294.","productDescription":"80 p.","numberOfPages":"94","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318261,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr70294.JPG"},{"id":287436,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0294/report.pdf"}],"country":"United States","state":"Iowa","county":"Linn","otherGeospatial":"Hoosier Creek, South Hoosier Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.835262,41.859836 ], [ -91.835262,42.299063 ], [ -91.363263,42.299063 ], [ -91.363263,41.859836 ], [ -91.835262,41.859836 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df8a0","contributors":{"authors":[{"text":"Schwob, Harlan H.","contributorId":23974,"corporation":false,"usgs":true,"family":"Schwob","given":"Harlan","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":192020,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38734,"text":"pp627D - 1970 - Urbanization and its effect on the temperature of the streams on Long Island, New York","interactions":[{"subject":{"id":55865,"text":"ofr68214 - 1968 - Urbanization and its effect on the temperature of Long Island streams","indexId":"ofr68214","publicationYear":"1968","noYear":false,"title":"Urbanization and its effect on the temperature of Long Island streams"},"predicate":"SUPERSEDED_BY","object":{"id":38734,"text":"pp627D - 1970 - Urbanization and its effect on the temperature of the streams on Long Island, New York","indexId":"pp627D","publicationYear":"1970","noYear":false,"chapter":"D","title":"Urbanization and its effect on the temperature of the streams on Long Island, New York"},"id":1}],"lastModifiedDate":"2025-04-15T19:35:26.01386","indexId":"pp627D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"627","chapter":"D","title":"Urbanization and its effect on the temperature of the streams on Long Island, New York","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology and some effects of urbanization on Long Island, New York (Professional Paper 6267)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp627D","usgsCitation":"Pluhowski, E., 1970, Urbanization and its effect on the temperature of the streams on Long Island, New York: U.S. Geological Survey Professional Paper 627, 110 p., https://doi.org/10.3133/pp627D.","productDescription":"110 p.","costCenters":[],"links":[{"id":65593,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0627d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123118,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0627d/report-thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.82194273612976,\n              41.07786507528178\n            ],\n            [\n              -72.20943503836517,\n              41.2154243330921\n            ],\n            [\n              -73.59610391993449,\n              40.940017333637996\n            ],\n            [\n              -73.79358198591106,\n              40.79824207303625\n            ],\n            [\n              -73.86178655629323,\n              40.79599717030078\n            ],\n            [\n              -73.9096568448226,\n              40.794714334653065\n            ],\n            [\n              -73.93592195888237,\n              40.77675203289462\n            ],\n            [\n              -73.9668470125343,\n              40.739849931946566\n            ],\n            [\n              -73.97531962997304,\n              40.70999238292043\n            ],\n            [\n              -74.00624468362446,\n              40.699073376332024\n            ],\n            [\n              -74.02446081111779,\n              40.67819382271807\n            ],\n            [\n              -74.05199681779393,\n              40.62451943874552\n            ],\n            [\n              -74.00158426558416,\n              40.54988209243214\n            ],\n            [\n              -73.92660160125092,\n              40.526379869031246\n            ],\n            [\n              -73.0763843222474,\n              40.624838818992174\n            ],\n            [\n              -72.36934591632716,\n              40.86170639680046\n            ],\n            [\n              -71.84784461657901,\n              41.0482487530538\n            ],\n            [\n              -71.82194273612976,\n              41.07786507528178\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60524e","contributors":{"authors":[{"text":"Pluhowski, E.J.","contributorId":52244,"corporation":false,"usgs":true,"family":"Pluhowski","given":"E.J.","affiliations":[],"preferred":false,"id":220363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67990,"text":"ha393 - 1970 - Floods on Rock River in northern Rock County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-05T14:28:29","indexId":"ha393","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"393","title":"Floods on Rock River in northern Rock County, Wisconsin","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha393","usgsCitation":"Shearman, J.O., 1970, Floods on Rock River in northern Rock County, Wisconsin: U.S. Geological Survey Hydrologic Atlas 393, 1 Sheet: 41.00 x 39.50 inches, https://doi.org/10.3133/ha393.","productDescription":"1 Sheet: 41.00 x 39.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":186361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89232,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/393/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"6000","country":"United States","state":"Wisconsin","county":"Rock County","otherGeospatial":"Rock River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.11749999999999,42.75 ], [ -89.11749999999999,42.833333333333336 ], [ -89,42.833333333333336 ], [ -89,42.75 ], [ -89.11749999999999,42.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df826","contributors":{"authors":[{"text":"Shearman, James O.","contributorId":95048,"corporation":false,"usgs":true,"family":"Shearman","given":"James","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":277462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56001,"text":"ofr70137 - 1970 - Neutron-activation analysis applied to hydrologic investigations","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"ofr70137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-137","title":"Neutron-activation analysis applied to hydrologic investigations","language":"ENGLISH","doi":"10.3133/ofr70137","usgsCitation":"Goldberg, M.C., Gottschall, C., and Janger, V., 1970, Neutron-activation analysis applied to hydrologic investigations: U.S. Geological Survey Open-File Report 70-137, 5 p., 3 figs., https://doi.org/10.3133/ofr70137.","productDescription":"5 p., 3 figs.","costCenters":[],"links":[{"id":181579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697ac1","contributors":{"authors":[{"text":"Goldberg, M. C.","contributorId":89220,"corporation":false,"usgs":true,"family":"Goldberg","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":254626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gottschall, C.W.","contributorId":75223,"corporation":false,"usgs":true,"family":"Gottschall","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":254625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Janger, V.J.","contributorId":12923,"corporation":false,"usgs":true,"family":"Janger","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":254624,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56005,"text":"ofr70151 - 1970 - Hydrologic studies of small watersheds, Green Creek, Brazos River basin, Texas, 1955-66","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"ofr70151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-151","title":"Hydrologic studies of small watersheds, Green Creek, Brazos River basin, Texas, 1955-66","language":"ENGLISH","doi":"10.3133/ofr70151","usgsCitation":"Hampton, B., 1970, Hydrologic studies of small watersheds, Green Creek, Brazos River basin, Texas, 1955-66: U.S. Geological Survey Open-File Report 70-151, 134 p., 23 figs., https://doi.org/10.3133/ofr70151.","productDescription":"134 p., 23 figs.","costCenters":[],"links":[{"id":181684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9d2","contributors":{"authors":[{"text":"Hampton, B.B.","contributorId":43362,"corporation":false,"usgs":true,"family":"Hampton","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":254631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67944,"text":"ha365 - 1970 - Water resources of southern Maryland","interactions":[],"lastModifiedDate":"2012-02-10T00:11:13","indexId":"ha365","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"365","title":"Water resources of southern Maryland","language":"ENGLISH","doi":"10.3133/ha365","isbn":"0607763671","usgsCitation":"Weigle, J.M., Webb, W.E., and Gardner, R.A., 1970, Water resources of southern Maryland: U.S. Geological Survey Hydrologic Atlas 365, 3 col. maps fold. in envelope 31 x 24 cm., https://doi.org/10.3133/ha365.","productDescription":"3 col. maps fold. in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":190319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89152,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/365/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89153,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/365/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89154,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/365/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.25,38.018055555555556 ], [ -77.25,38.75 ], [ -76.26805555555555,38.75 ], [ -76.26805555555555,38.018055555555556 ], [ -77.25,38.018055555555556 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f066a","contributors":{"authors":[{"text":"Weigle, James Montgomery","contributorId":59479,"corporation":false,"usgs":true,"family":"Weigle","given":"James","email":"","middleInitial":"Montgomery","affiliations":[],"preferred":false,"id":277364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Webb, Wayne Eldredge","contributorId":66355,"corporation":false,"usgs":true,"family":"Webb","given":"Wayne","email":"","middleInitial":"Eldredge","affiliations":[],"preferred":false,"id":277365,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, Richard Alfred","contributorId":89134,"corporation":false,"usgs":true,"family":"Gardner","given":"Richard","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":277366,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13941,"text":"ofr71140 - 1970 - Geologic evaluation of 3-5 micrometer infrared imagery and color photography in southern Utah","interactions":[],"lastModifiedDate":"2026-04-22T15:41:28.025693","indexId":"ofr71140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"71-140","title":"Geologic evaluation of 3-5 micrometer infrared imagery and color photography in southern Utah","docAbstract":"<p>A comparison of 3-5 micrometer, afternoon and midnight infrared (IR) imagery and color photography with conventional aerial photography shows that IR imagery and color photography have some unique capabilities. In general, the IR imagery provides in shades of gray a record of the relative ground temperature at the time the image was taken. It has day or night capabilities for imaging large areas of terrain. In sparsely vegetated areas, midnight IR imagery shows some tonal variations that may be relate to specific rock type based on temperature differences. In heavily vegetated areas, any temperature difference that might exist between rock units is masked by the temperature difference associated with different vegetation communities; although, isolated outcrops in such areas are generally apparent because they are brighter (warmer) on the afternoon IR. On the midnight IR they may or may not be brighter according to their differences in thermal inertia. The afternoon IR image showed one fault that was not visible on the aerial photographs. In contrast, only some of the faults visible in the stereoscopic model were recognized on the IR imagery. The interpreter using IR imagery must be aware of changes in heat patterns resulting from modification of the land by man and from the effect of cloud shadows. Apparent anomalies on IR image resulting from such factors might be misinterpreted. Compared to conventional photography with the added ability of stereoscopic viewing the day and night IR provided less geologic information in the area of study. IR imagery may be useful in hydrologic studies such as the relative temperatures of alpine lakes, ponds, and marshes during the night. and day. It should prove valuable in ecological studies involving the relative temperatures of different plant communities. Roads in heavily wooded areas are easier to see on the IR image, than on conventional photography because of their temperature differences.</p><p>Color photography, as might be expected, shows the terrain in a close approximation to its natural color, and delineates some stratigraphic units and rock alterations that are indistinguishable on black and white photography.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71140","usgsCitation":"Hackman, R., and Williams, P., 1970, Geologic evaluation of 3-5 micrometer infrared imagery and color photography in southern Utah: U.S. Geological Survey Open-File Report 71-140, iii, 43 leaves :ill., maps ;27 cm., https://doi.org/10.3133/ofr71140.","productDescription":"iii, 43 p.","costCenters":[],"links":[{"id":503306,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147079,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0140/report-thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA  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Robert J.","contributorId":30999,"corporation":false,"usgs":true,"family":"Hackman","given":"Robert J.","affiliations":[],"preferred":false,"id":168676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":168677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39674,"text":"pp627C - 1970 - Preliminary results of hydrologic studies at two recharge basins on Long Island, New York","interactions":[],"lastModifiedDate":"2025-04-15T19:33:19.796398","indexId":"pp627C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"627","chapter":"C","title":"Preliminary results of hydrologic studies at two recharge basins on Long Island, New York","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology and some effects of urbanization on Long Island, New York (Professional Paper 627)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp627C","usgsCitation":"Seaburn, G., 1970, Preliminary results of hydrologic studies at two recharge basins on Long Island, New York: U.S. Geological Survey Professional Paper 627, 17 p., https://doi.org/10.3133/pp627C.","productDescription":"17 p.","costCenters":[],"links":[{"id":67397,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0627c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122167,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0627c/report-thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.82194273612976,\n              41.07786507528178\n            ],\n            [\n              -72.20943503836517,\n              41.2154243330921\n            ],\n            [\n              -73.59610391993449,\n              40.940017333637996\n            ],\n            [\n              -73.79358198591106,\n              40.79824207303625\n            ],\n            [\n              -73.86178655629323,\n              40.79599717030078\n            ],\n            [\n              -73.9096568448226,\n              40.794714334653065\n            ],\n            [\n              -73.93592195888237,\n              40.77675203289462\n            ],\n            [\n              -73.9668470125343,\n              40.739849931946566\n            ],\n            [\n              -73.97531962997304,\n              40.70999238292043\n            ],\n            [\n              -74.00624468362446,\n              40.699073376332024\n            ],\n            [\n              -74.02446081111779,\n              40.67819382271807\n            ],\n            [\n              -74.05199681779393,\n              40.62451943874552\n            ],\n            [\n              -74.00158426558416,\n              40.54988209243214\n            ],\n            [\n              -73.92660160125092,\n              40.526379869031246\n            ],\n            [\n              -73.0763843222474,\n              40.624838818992174\n            ],\n            [\n              -72.36934591632716,\n              40.86170639680046\n            ],\n            [\n              -71.84784461657901,\n              41.0482487530538\n            ],\n            [\n              -71.82194273612976,\n              41.07786507528178\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b2be","contributors":{"authors":[{"text":"Seaburn, G.E.","contributorId":42193,"corporation":false,"usgs":true,"family":"Seaburn","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":221957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55999,"text":"ofr70135 - 1970 - Summary of ground-water hydrological data in Michigan in 1968","interactions":[],"lastModifiedDate":"2017-07-12T10:31:57","indexId":"ofr70135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-135","title":"Summary of ground-water hydrological data in Michigan in 1968","docAbstract":"<p>The purpose of this report is to make available the records of groundwater levels in the principal aquifers of the State through 1968 and to compile other related data, such as records of ground-water pumpage, data on municipal, public and industrial water-supply facilities, and the effects of precipitation on ground-water levels. Records of water levels in areas of heavy pumpage and in areas where changes are principally from natural influences are illustrated or tabulated to allow comparison between these types of water-level fluctuations. The water-levels and related data provide a day-to-day record for the evaluation of available ground-water supplies. The long-term records serve as a framework to which short-term records may be related.</p><p>This report is written for those persons, municipalities, industries, institutions, consultants, drillers and hydrologists interested in the groundwater resources of the State.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70135","usgsCitation":"Giroux, P., and Huffman, G., 1970, Summary of ground-water hydrological data in Michigan in 1968: U.S. Geological Survey Open-File Report 70-135, vii, 105 p., https://doi.org/10.3133/ofr70135.","productDescription":"vii, 105 p.","numberOfPages":"115","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":55992,"text":"ofr70114 - 1970 - A national hydrologic data system for Chile","interactions":[],"lastModifiedDate":"2012-02-02T00:12:11","indexId":"ofr70114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-114","title":"A national hydrologic data system for Chile","language":"ENGLISH","doi":"10.3133/ofr70114","usgsCitation":"Doyel, W., and Moss, M.E., 1970, A national hydrologic data system for Chile: U.S. Geological Survey Open-File Report 70-114, 141 p., 1 fig., https://doi.org/10.3133/ofr70114.","productDescription":"141 p., 1 fig.","costCenters":[],"links":[{"id":184850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade18","contributors":{"authors":[{"text":"Doyel, W.W.","contributorId":74818,"corporation":false,"usgs":true,"family":"Doyel","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":254608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moss, M. E.","contributorId":50500,"corporation":false,"usgs":true,"family":"Moss","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":254607,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32768,"text":"pp427C - 1970 - Influences of strip mining on the hydrologic environment of parts of Beaver Creek basin, Kentucky, 1955-66","interactions":[],"lastModifiedDate":"2018-03-13T17:47:23","indexId":"pp427C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"427","chapter":"C","title":"Influences of strip mining on the hydrologic environment of parts of Beaver Creek basin, Kentucky, 1955-66","docAbstract":"<p>This report is the third of a series on the environmental effects of strip mining of coal in Cane Branch basin, McCreary County, Ky. The series of reports, which is being published by the U.S. Geological Survey as Professional Paper 427, is the product of a cooperative study by several Federal and State agencies. The physical environment of the study areas and the history of mining in the basin are described in the first report, Professional Paper 427-A (Musser, 1963). Results obtained during the study period 1955-59 and definitions of terms are given in the second report, Professional Paper 427-B (Collier and others, 1964). The present report describes the results of the investigation since 1955, with emphasis on the period 1959-66.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp427C","collaboration":"Prepared in collaboration with the U.S. Department of the Interior, Bureau of Sport Fisheries and Wildlife; U.S. Department of Agriculture, Forest Service and Soil Conservation Service; Department of the Army, Corps of Engineers; and Commonwealth of Kentucky, University of Kentucky and Department of Fish and Wildlife Resources","usgsCitation":"1970, Influences of strip mining on the hydrologic environment of parts of Beaver Creek basin, Kentucky, 1955-66: U.S. Geological Survey Professional Paper 427, 80 p., https://doi.org/10.3133/pp427C.","productDescription":"80 p.","startPage":"C1","endPage":"C80","costCenters":[],"links":[{"id":121587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0427c/report-thumb.jpg"},{"id":60705,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60706,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60707,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0427c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db3f","contributors":{"editors":[{"text":"Collier, C. R.","contributorId":22033,"corporation":false,"usgs":true,"family":"Collier","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":731010,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Pickering, R.J.","contributorId":103253,"corporation":false,"usgs":true,"family":"Pickering","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":731011,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Musser, J.J.","contributorId":72035,"corporation":false,"usgs":true,"family":"Musser","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":731012,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}}
,{"id":68466,"text":"ha428 - 1970 - Ground-water resources of Nelson County, northeastern North Dakota","interactions":[],"lastModifiedDate":"2018-03-21T16:25:32","indexId":"ha428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"428","title":"Ground-water resources of Nelson County, northeastern North Dakota","docAbstract":"<p>This investigation is part of a Statewide program to determine the location and extent of the ground-water reservoirs (aquifers); to evaluate the occurrence and movement of ground water within these aquifers, including the sources of recharge and discharge; and to determine the chemical quality of the ground water.</p><p>Nelson County covers an area of approximately 1,000 square miles in northeastern North Dakota.&nbsp; The study, which began in July 1967, has been made cooperatively by the U.S. Geological Survey, the North Dakota State Water Commission, the North Dakota Geological Survey, and the Nelson County Water Management District.&nbsp; The final results of the study will be published in three parts by the cooperating State agencies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha428","usgsCitation":"Downey, J.S., 1970, Ground-water resources of Nelson County, northeastern North Dakota: U.S. Geological Survey Hydrologic Atlas 428, 28.28 x 29.48 inches, https://doi.org/10.3133/ha428.","productDescription":"28.28 x 29.48 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":188627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":276308,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/428/plate-1.pdf"}],"scale":"26720","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5,47.833333333333336 ], [ -98.5,48.166666666666664 ], [ -98,48.166666666666664 ], [ -98,47.833333333333336 ], [ -98.5,47.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5e2","contributors":{"authors":[{"text":"Downey, Joe S.","contributorId":102454,"corporation":false,"usgs":true,"family":"Downey","given":"Joe","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":278282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56000,"text":"ofr70136 - 1970 - Summary of ground-water hydrological data in Michigan in 1969","interactions":[],"lastModifiedDate":"2017-07-12T10:30:30","indexId":"ofr70136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-136","title":"Summary of ground-water hydrological data in Michigan in 1969","docAbstract":"<p>The purpose of this report is to make available the records of ground-water levels in the principal aquifers of the State through 1969 and to compile other related data, such as records of groundwater pumpage, data on municipal, public and industrial water-supply facilities, and the effects of precipitation on ground-water levels. Records of water levels in areas of heavy pumpage, and in areas where changes are principally from natural influences, are illustrated or tabulated to allow comparison between these types of water-level fluctuations. The water levels and related data provide a day-to-day record for the evaluation of available ground-water supplies. The long-term records serve as a framework to which short-term records may be related.</p><p>This report is written for those persons, municipalities, industries, institutions, consultants, drillers, and hydrologists interested in the ground-water resources of the State.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70136","usgsCitation":"Giroux, P., and Huffman, G., 1970, Summary of ground-water hydrological data in Michigan in 1969: U.S. Geological Survey Open-File Report 70-136, vii, 101 p., https://doi.org/10.3133/ofr70136.","productDescription":"vii, 101 p.","numberOfPages":"113","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":48003,"text":"ofr71266 - 1970 - A plan for water-resources investigations in Arkansas, with definitions of hydrologic units","interactions":[],"lastModifiedDate":"2012-02-02T00:10:08","indexId":"ofr71266","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"71-266","title":"A plan for water-resources investigations in Arkansas, with definitions of hydrologic units","language":"ENGLISH","doi":"10.3133/ofr71266","usgsCitation":"Sniegocki, R., and Bedinger, M.S., 1970, A plan for water-resources investigations in Arkansas, with definitions of hydrologic units: U.S. Geological Survey Open-File Report 71-266, 70 p., https://doi.org/10.3133/ofr71266.","productDescription":"70 p.","costCenters":[],"links":[{"id":161896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0266/report-thumb.jpg"},{"id":84780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0266/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84781,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0266/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84782,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0266/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84783,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0266/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84784,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0266/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84785,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0266/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84786,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0266/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab6e2","contributors":{"authors":[{"text":"Sniegocki, R. T.","contributorId":38546,"corporation":false,"usgs":true,"family":"Sniegocki","given":"R. T.","affiliations":[],"preferred":false,"id":236659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":236660,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22641,"text":"ofr7051 - 1970 - Flood of August 1969 in Virginia","interactions":[],"lastModifiedDate":"2019-02-05T07:55:42","indexId":"ofr7051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-51","title":"Flood of August 1969 in Virginia","docAbstract":"<p>Hurricane Camille became a tropical depression and soaked central Virginia with up to 28 inches of rain during the night of August 19th and morning of the 20th. The rains, flash floods, and rain-induced landslides accompanying the storm's passage have been called the worst natural disaster ever to strike Virginia.</p><p>Discharge of streams in the James, Potomac, Rappahapnock, and York River basins exceeded previous known maximums. At Tye River near Lovingston the peak flood discharge was eight times the previous high during the 31 years of record. James River stations downstream from the Maury River recorded peak flows of greater than 100-year recurrence interval.</p><p>As of Nov. 13, 1969, the State had counted 113 dead and 102 injured with 39 persons still missing. The total damage amounted to over $116 million.</p><p>This report provides hydrologic data needed for planning and design. The report includes a general description of the flood; precipitation information; sediment aspects of the flood; and records of stage and/or discharge for 105 sites. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7051","issn":"0094-9140","collaboration":"Prepared in cooperation with the State of Virginia","usgsCitation":"Camp, J., and Miller, E., 1970, Flood of August 1969 in Virginia: U.S. Geological Survey Open-File Report 70-51, Report: x, 120 p.; 1 Plate: 36.16 x 19.43 inches, https://doi.org/10.3133/ofr7051.","productDescription":"Report: x, 120 p.; 1 Plate: 36.16 x 19.43 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eee94","contributors":{"authors":[{"text":"Camp, J.D.","contributorId":61855,"corporation":false,"usgs":true,"family":"Camp","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":188622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, E.M.","contributorId":42215,"corporation":false,"usgs":true,"family":"Miller","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":188621,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68341,"text":"ha379 - 1970 - Reconnaissance bathymetry of Pyramid Lake, Washoe County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"ha379","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"379","title":"Reconnaissance bathymetry of Pyramid Lake, Washoe County, Nevada","language":"ENGLISH","doi":"10.3133/ha379","usgsCitation":"Harris, E., 1970, Reconnaissance bathymetry of Pyramid Lake, Washoe County, Nevada: U.S. Geological Survey Hydrologic Atlas 379, 1 map., https://doi.org/10.3133/ha379.","productDescription":"1 map.","costCenters":[],"links":[{"id":190415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89817,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/379/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.75,39.75 ], [ -119.75,40.25 ], [ -119.25,40.25 ], [ -119.25,39.75 ], [ -119.75,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64475e","contributors":{"authors":[{"text":"Harris, E. E.","contributorId":24328,"corporation":false,"usgs":true,"family":"Harris","given":"E. E.","affiliations":[],"preferred":false,"id":278064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22805,"text":"ofr7093 - 1970 - Water resources in the Big Lost River Basin, south-central Idaho","interactions":[],"lastModifiedDate":"2013-11-19T10:42:50","indexId":"ofr7093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"70-93","title":"Water resources in the Big Lost River Basin, south-central Idaho","docAbstract":"The Big Lost River basin occupies about 1,400 square miles in south-central Idaho and drains to the Snake River Plain. The economy in the area is based on irrigation agriculture and stockraising. The basin is underlain by a diverse-assemblage of rocks which range, in age from Precambrian to Holocene. The assemblage is divided into five groups on the basis of their hydrologic characteristics. Carbonate rocks, noncarbonate rocks, cemented alluvial deposits, unconsolidated alluvial deposits, and basalt. The principal aquifer is unconsolidated alluvial fill that is several thousand feet thick in the main valley. The carbonate rocks are the major bedrock aquifer. They absorb a significant amount of precipitation and, in places, are very permeable as evidenced by large springs discharging from or near exposures of carbonate rocks. Only the alluvium, carbonate rock and locally the basalt yield significant amounts of water. \n\nA total of about 67,000 acres is irrigated with water diverted from the Big Lost River. The annual flow of the river is highly variable and water-supply deficiencies are common. About 1 out of every 2 years is considered a drought year. In the period 1955-68, about 175 irrigation wells were drilled to provide a supplemental water supply to land irrigated from the canal system and to irrigate an additional 8,500 acres of new land.\n\nAverage. annual precipitation ranged from 8 inches on the valley floor to about 50 inches at some higher elevations during the base period 1944-68. The estimated water yield of the Big Lost River basin averaged 650 cfs (cubic feet per second) for the base period. Of this amount, 150 cfs was transpired by crops, 75 cfs left the basin as streamflow, and 425 cfs left as ground-water flow. A map of precipitation and estimated values of evapotranspiration were used to construct a water-yield map. \n\nA distinctive feature of the Big Lost River basin, is the large interchange of water from surface streams into the ground and from the ground into the surface streams. Large quantities of water disappear in the Chilly, Darlington, and other sinks and reappear above Mackay Narrows, above Moore Canal heading, and in other reaches. A cumulative summary of water yield upstream from selected points in the basin is as follows :\n\nAbove Howell Ranch: water yield: 345 cfs; surface water: 310 cfs; ground water: 35 cfs\n\nAbove. Mackay Narrows water yield: 450 cfs; surface water: 325 cfs; ground water: 75 cfs; crop evapotranspiration: 50 cfs\n\nAbove Arco: water yield: 650 cfs; surface water: 75 cfs; ground water: 425 cfs; crop evapotranspiration: 150 cfs\n\nGround-water pumping affects streamflow in reaches , where the stream and water table are continuous, but the effects of pumping were not measured except locally. Pumping depletes the total water supply by the. amount of the pumped water that is evapotranspired by crops. The part of the pumped water that is not consumed percolates into the ground or runs off over the land surface to the stream. The estimated 425 cfs that leaves the basin as ground-water flow is more than adequate for present and foreseeable needs. However because much of the outflow occurs at considerable depth, the quantity that is salvageable is unknown.\n\nBoth the surface and ground waters are of good quality and are suitable for most uses. Although these waters are low in total dissolved solids, they tend to be hard or very hard.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7093","collaboration":"Prepared in cooperation with the Idaho Department of Reclamation","usgsCitation":"Crosthwaite, E., Thomas, C., and Dyer, K., 1970, Water resources in the Big Lost River Basin, south-central Idaho: U.S. Geological Survey Open-File Report 70-93, vi, 109 p., https://doi.org/10.3133/ofr7093.","productDescription":"vi, 109 p.","numberOfPages":"122","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0093/report-thumb.jpg"},{"id":52236,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Big Lost River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.112216,43.516533 ], [ -113.112216,44.096 ], [ -114.119915,44.096 ], [ -114.119915,43.516533 ], [ -113.112216,43.516533 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f09e0","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":188905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, C.A.","contributorId":14385,"corporation":false,"usgs":true,"family":"Thomas","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":188904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dyer, K.L.","contributorId":100011,"corporation":false,"usgs":true,"family":"Dyer","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":188906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68309,"text":"ha376 - 1970 - Sediment yields of Wisconsin streams","interactions":[],"lastModifiedDate":"2015-10-06T07:48:35","indexId":"ha376","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"376","title":"Sediment yields of Wisconsin streams","docAbstract":"<p><span>Sediment in Wisconsin streams causes economic and engineering problems in water management and reduces the value of water for nearly all uses. Sediment produces problems such as reduced reservoir capacity, navigation hazards, increased cost of water treatment, property damage, temporary loss of farmland, destruction of feeding and nesting grounds of fish, and destruction of wildlife habitat. Sediment in water also reduces the aesthetic value of surface waters and is detrimental to the State's tourist and recreation industry.</span></p>\n<p><span>The yield of sediment from a drainage basin is subject to many environmental influences. Most sediment results from the weathering and erosion of soil and rock materials. Other factors such as rainfall intensity, runoff rate, topography, rock type, soil characteristics, vegetal cover, and land use also influence the rate of sediment production and movement. An understanding of the many parameters that influence sediment yield is a basic need for managing the State's water resources.</span></p>\n<p><span>The purpose of this report is to describe the magnitude and variability of sediment in Wisconsin streams, to relate sediment yields to the local environment, and to identify areas that need further study. The report is based on sediment data from 44 stream-gaging sites throughout the State. Determination of local areas of erosion and deposition are beyond the scope of the report.</span></p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha376","usgsCitation":"Hindall, S.M., and Flint, R., 1970, Sediment yields of Wisconsin streams: U.S. Geological Survey Hydrologic Atlas 376, 1 Sheet: 35.50 x 35.00 inches, https://doi.org/10.3133/ha376.","productDescription":"1 Sheet: 35.50 x 35.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":185690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89753,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/376/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United 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